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邵于庄煤炭勘查区新生界松散层水文地质特征
引用本文:云晓鸣,高艳,李云峰.邵于庄煤炭勘查区新生界松散层水文地质特征[J].中国煤炭地质,2008(12):53-54.
作者姓名:云晓鸣  高艳  李云峰
作者单位:安徽省煤田地质局第三勘探队
摘    要:邵于庄煤炭勘查区新生界松散层厚度较厚,下伏为二叠系含煤地层,可采煤层多。区内含、隔水层组成复杂,由四个含水层和三个隔水层组成。通过对含水层水文地质条件分析,提出了第一、二含水层是矿区的主要供水水源,为保证未来建设和开采时的生活用水和工业用水,应做好水源的保护工作;同时指明了第四含水层是浅部煤组开采的主要补给水源,在煤矿设计和开采过程中,应重点予以防治。

关 键 词:含水层  隔水层  新生界  邵于庄煤炭勘查区

Shaoyuzhuang Coal Exploration Area Cenozoic Loose Bed Hydrogeological Characteristics
Yun Xiaoming,Gao Yan and Li Yunfeng.Shaoyuzhuang Coal Exploration Area Cenozoic Loose Bed Hydrogeological Characteristics[J].Coal Geology of China,2008(12):53-54.
Authors:Yun Xiaoming  Gao Yan and Li Yunfeng
Institution:(The Third Exploration Team, Anhui Bureau of Coal Geological Exploration, Suzhou, Anhui 234000)
Abstract:Cenozoic loose bed in the Shaoyuzhuang coal exploration area is rather thick.Underlying is the Permian coal-bearing strata with many mineable coal seams.There are 4 aquifers and 3 confining beds in the area.Through analyses of aquifer hydrogeological conditions,advised that the first and second aquifers should be the main water supply sources in the mining area.To ensure water for living and industrial use,water source protection ought to think much of.Meanwhile pointed out that the Quaternary aquifer is the main recharging source of shallow coal groups,thus should be careful about in coalmine design and coal mining.
Keywords:aquifer  confining bed  Cenozoic Erathem  Shaoyuzhuang coal exploration area  
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